Julien Siebert

Université Paris-Saclay

France

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Articles (10)

Year:

2021

Year:

2021

Year:

2021

Year:

2021

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2020

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2020

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2020

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2020

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2020

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2020

Collaborators (4)

Paolo Angelo Sossi

Assistant Professor

ETH Zürich

SWITZERLAND

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Paul Savage

University of St. Andrews

UNITED KINGDOM

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Frederic Moynier

FRANCE

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Guillaume Fiquet

CNRS Délégation Paris B

FRANCE

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Julien Siebert

Research Interests

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Articles (10)

Reconciling metal–silicate partitioning and late accretion in the Earth

Earth's volatile accretion as told by Cd, Bi, Sb and Tl core–mantle distribution

Quantitative estimates of impact induced crustal erosion during accretion and its influence on the Sm/Nd ratio of the Earth

Tidal pull of the Earth strips the proto-Moon of its volatiles

An experimentally-determined general formalism for evaporation and isotope fractionation of Cu and Zn from silicate melts between 1300 and 1500 °C and 1 bar

Metal-silicate silicon isotopic fractionation and the composition of the bulk Earth

A new reference for the thermal equation of state of iron

Early oxidation of the martian crust triggered by impacts

Iron isotope evidence for very rapid accretion and differentiation of the proto-Earth

The niobium and tantalum concentration in the mantle constrains the composition of Earth’s primordial magma ocean

Collaborators (4)

Paolo Angelo Sossi

Paul Savage

Frederic Moynier

Guillaume Fiquet

Make your next move.

Julien Siebert

Research Interests

Explore related searches

Contact this professor

Articles (10)

Reconciling metal–silicate partitioning and late accretion in the Earth

Earth's volatile accretion as told by Cd, Bi, Sb and Tl core–mantle distribution

Quantitative estimates of impact induced crustal erosion during accretion and its influence on the Sm/Nd ratio of the Earth

Tidal pull of the Earth strips the proto-Moon of its volatiles

An experimentally-determined general formalism for evaporation and isotope fractionation of Cu and Zn from silicate melts between 1300 and 1500 °C and 1 bar

Metal-silicate silicon isotopic fractionation and the composition of the bulk Earth

A new reference for the thermal equation of state of iron

Early oxidation of the martian crust triggered by impacts

Iron isotope evidence for very rapid accretion and differentiation of the proto-Earth

The niobium and tantalum concentration in the mantle constrains the composition of Earth’s primordial magma ocean

Collaborators (4)

Paolo Angelo Sossi

Paul Savage

Frederic Moynier

Guillaume Fiquet

Make your next move.

An experimentally-determined general formalism for evaporation and isotope fractionation of Cu and Zn from silicate melts between 1300 and 1500 °C and 1 bar